Impact of two typhoons on the marine environment in the Yellow Sea and East China Sea

Dongyang Fu; Hong Luan; Delu Pan; Ying Zhang; Li’an Wang; Dazhao Liu; Youzhuan Ding; Xue Li

doi:10.1007/s00343-016-5049-6

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Impact of two typhoons on the marine environment in the Yellow Sea and East China Sea

Updated：2023-05-16

- Impact of two typhoons on the marine environment in the Yellow Sea and East China Sea
- Journal of Oceanology and Limnology Vol. 34, Issue 4, Pages: 871-884(2016)
- Affiliations：
  
  1. Lab of Remote Sensing & Information Technology Guangdong Ocean University
  2. State Key Laboratory of Satellite Ocean Environment Dynamics (Second Institute of Oceanography State Oceanic Administration)
- Author bio：
- Funds：
- DOI：10.1007/s00343-016-5049-6
  CLC：
- Online First：07 January 2016，
  
  Published：2016
- Accepted：
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Fu, D., Luan, H., Pan, D. et al. Impact of two typhoons on the marine environment in the Yellow Sea and East China Sea., Chin. J. Ocean. Limnol. 34, 871–884 (2016). https://doi.org/10.1007/s00343-016-5049-6
DOI：

Fu, D., Luan, H., Pan, D. et al. Impact of two typhoons on the marine environment in the Yellow Sea and East China Sea., Chin. J. Ocean. Limnol. 34, 871–884 (2016). https://doi.org/10.1007/s00343-016-5049-6 DOI：

摘要

Abstract

This study investigated the effects of two typhoons (Nari and Wipha) on sea surface temperature (SST) and chlorophyll-a (Chl-a) concentration. Typhoons Nari and Wipha passed through the Yellow Sea on September 13

2007 and the East China Sea (ECS) on September 16

2007

respectively. The SST and Chl-a data were obtained from the Aqua/Terra MODIS and NOAA18

respectively

and the temperature and salinity in the southeast of the study area were observed in situ from Argo. The average SST within the study area dropped from 26.33°C on September 10 to a minimum of 22.79°C on September 16. Without the usual phenomenon of ‘right bias’

the most striking response of SST was in the middle of the typhoons’ tracks

near to coastal waters. Strong cooling of the upper layers of the water column was probably due to increased vertical mixing

discharge from the Changjiang River estuary

and heavy rainfall. During the typhoons

average Chl-a increased by 11.54% within the study area and by 21.69% in the offshore area near to the southeast ECS. From September 1 to 13

average Chl-a was only 0.10 mg/m3 in the offshore waters but it reached a peak of >0.17 mg/m3 on September 18. This large increase in Chl-a concentration in offshore waters might have been triggered by strong vertical mixing

upwelling induced by strong typhoons

and sedimentation and nutrient influx following heavy rainfall.

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Keywords

references

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